Preprints
https://doi.org/10.5194/egusphere-2023-1498
https://doi.org/10.5194/egusphere-2023-1498
11 Jul 2023
 | 11 Jul 2023

The fate of fixed nitrogen in Santa Barbara Basin sediments during seasonal anoxia

Xuefeng Peng, David J. Yousavich, Annie Bourbonnais, Frank Wenzhoefer, Felix Janssen, Tina Treude, and David L. Valentine

Abstract. Despite long-standing interests in the biogeochemistry of the Santa Barbara Basin (SBB), there are no direct rate measurements of different nitrogen transformation processes. We investigated benthic nitrogen cycling using in-situ incubations with 15NO3- addition and quantified the rates of total nitrate (NO3-) uptake, denitrification, anaerobic ammonia oxidation (anammox), N2O production, and dissimilatory nitrate reduction to ammonia (DNRA). Denitrification was the dominant NO3- reduction process, while anammox contributed 0–27 % to total NO3- reduction. DNRA accounted for less than half of NO3- reduction except at the deepest station at the center of the SBB where NO3- concentration was lowest. NO3- availability and sediment total organic carbon content appeared to be two key controls on the relative importance of DNRA. The negative correlation between NO3- availability and the relative importance of DNRA suggests a negative feedback loop that potentially contributes to stabilizing the fixed N budget in the SBB. Nitrous oxide (N2O) production as a fraction of total NO3- reduction ranged from 0.2 % to 1.5 %, which was higher than previous reports from nearby borderland basins. A large fraction of NO3- uptake was unaccounted for by NO3- reduction processes, suggesting that intracellular storage may play an important role. Our results indicate that the SBB acts as a strong sink for fixed nitrogen and potentially a net source of N2O to the water column.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Xuefeng Peng, David J. Yousavich, Annie Bourbonnais, Frank Wenzhoefer, Felix Janssen, Tina Treude, and David L. Valentine

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1498', Anonymous Referee #1, 11 Mar 2024
    • AC1: 'Reply on RC1', Xuefeng Peng, 29 Mar 2024
  • RC2: 'Comment on egusphere-2023-1498', Anonymous Referee #2, 15 Mar 2024
    • AC2: 'Reply on RC2', Xuefeng Peng, 29 Mar 2024

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1498', Anonymous Referee #1, 11 Mar 2024
    • AC1: 'Reply on RC1', Xuefeng Peng, 29 Mar 2024
  • RC2: 'Comment on egusphere-2023-1498', Anonymous Referee #2, 15 Mar 2024
    • AC2: 'Reply on RC2', Xuefeng Peng, 29 Mar 2024
Xuefeng Peng, David J. Yousavich, Annie Bourbonnais, Frank Wenzhoefer, Felix Janssen, Tina Treude, and David L. Valentine
Xuefeng Peng, David J. Yousavich, Annie Bourbonnais, Frank Wenzhoefer, Felix Janssen, Tina Treude, and David L. Valentine

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Short summary
Biologically available (fixed) nitrogen (N) is a limiting nutrient for life in the ocean. Under low oxygen conditions, fixed N is either removed via denitrification or retained via dissimilatory nitrate reduction to ammonia (DNRA). Using in-situ incubations in the Santa Barbara Basin which undergoes seasonal anoxia, we found that benthic denitrification was the dominant nitrate reduction process, while nitrate availability and organic matter content control the relative importance of DNRA.